3.1 Section Objectives – page 65  Identify some common limiting factors. Section Objectives:  Explain how limiting factors and ranges of tolerance affect distribution of organisms.  Sequence the stages of ecological succession.  Describe the conditions under which primary and secondary succession take place.

Section 3.1 Summary – pages  Various combinations of abiotic and biotic factors interact in different places around the world. Life in a Community

Section 3.1 Summary – pages  The result is that conditions in one part of the world are suitable for supporting certain forms of life, but not others. Life in a Community

Section 3.1 Summary – pages  Factors that affect an organism’s ability to survive in its environment, such as the availability of water and food, predators, and temperature, are called limiting factors. Limiting factors

Section 3.1 Summary – pages  A limiting factor is any biotic or abiotic factor that restricts the existence, numbers, reproduction, or distribution of organisms. Common Limiting Factors Sunlight Climate Atmospheric gases Temperature Water Nutrients/Food Fire Soil chemistry Space Other organisms Limiting factors

Section 3.1 Summary – pages Limiting factors  Factors that limit one population in a community may also have an indirect effect on another population.

Section 3.1 Summary – pages Ranges of tolerance  The ability of an organism to withstand fluctuations in biotic and abiotic environmental factors is known as tolerance. Limits of Tolerance Organisms absent Organisms infrequent Greatest number of organisms Organisms infrequent Organisms absent Zone of intolerance Zone of Physiological stress Optimum range Lower limitUpper limit Range of tolerance Population Zone of Physiological stress Zone of intolerance

Section 3.1 Summary – pages Succession: Changes over Time  Ecologists refer to the orderly, natural changes and species replacements that take place in the communities of an ecosystem as succession.  Succession occurs in stages. At each stage, different species of plants and animals may be present.

Section 3.1 Summary – pages Succession: Changes over Time  As succession progresses, new organisms move in.  Others may die out or move out.  There are two types of succession—primary and secondary.

Section 3.1 Summary – pages  The colonization of barren land by communities of organisms is called primary succession.  Primary succession takes place on land where there are no living organisms. Primary succession

Section 3.1 Summary – pages Primary succession  The first species to take hold in an area like this are called pioneer species.  An example of pioneer species is a lichen, which is a combination of small organisms.

Section 3.1 Summary – pages  Decaying lichens, along with bits of sediment in cracks and crevices of rock, make up the first stage of soil development.  New soil makes it possible for small weedy plants, small ferns, fungi, and insects to become established. Primary succession

Section 3.1 Summary – pages  As these organisms die, more soil builds. ­ Exposed rock Primary succession Moss Lichen Pioneer species Primary succession

Section 3.1 Summary – pages  After some time, primary succession slows down and the community becomes fairly stable, or reaches equilibrium. Primary succession

Section 3.1 Summary – pages  A stable, mature community that undergoes little or no change in species is a climax community. Secondary succession Climax community Primary succession

Section 3.1 Summary – pages Secondary succession  Secondary succession is the sequence of changes that takes place after an existing community is severely disrupted in some way.  Secondary succession, however, occurs in areas that previously contained life, and on land that still contains soil.

Section 3.1 Summary – pages Secondary succession  Because soil already exists, secondary succession may take less time than primary succession to reach a climax community.

3.2 Section Objectives – page 70  Compare and contrast the photic and aphotic zones of marine biomes. Section Objectives:  Identify the major limiting factors affecting distribution of terrestrial biomes.  Distinguish among biomes.

Section 3.2 Summary – pages  A biome is a large group of ecosystems that share the same type of climax community.  There are terrestrial biomes and aquatic biomes, each with organisms adapted to the conditions characteristic of the biome. What is a biome?

Section 3.2 Summary – pages What is a biome?  Biomes located on land are called terrestrial biomes.  Oceans, lakes, streams, ponds, or other bodies of water are aquatic biomes.

Section 3.2 Summary – pages Aquatic Biomes  Approximately 75 percent of Earth’s surface is covered with water.  Most of that water is salty.  Freshwater is confined to rivers, streams, ponds, and most lakes.  As a result, aquatic biomes are separated into marine biomes and freshwater biomes.

Section 3.2 Summary – pages  Different parts of the ocean differ in biotic and abiotic factors (salinity, depth, availability of light, and temperature) found there.  One of the ways ecologists study marine biomes is to make separate observations in shallow, sunlit zones and deeper, unlighted zones. Marine biomes

Section 3.2 Summary – pages Marine biomes  The portion of the marine biome that is shallow enough for sunlight to penetrate is called the photic zone.

Section 3.2 Summary – pages Marine biomes  Deeper water that never receives sunlight makes up the aphotic zone.

Section 3.2 Summary – pages  An estuary is a coastal body of water, partially surrounded by land, in which freshwater and salt water mix.  The salinity, or amount of salt, in an estuary ranges between that of seawater and that of freshwater, and depends on how much freshwater the river brings into the estuary. Estuaries—Mixed waters

Section 3.2 Summary – pages Estuaries—Mixed waters  Estuaries, may contain salt marsh ecosystems, which are dominated by salt-tolerant smooth cordgrass, salt marsh hay, or eelgrasses.

Section 3.2 Summary – pages  Daily, the gravitational pull of the sun and moon causes the rise and fall of ocean tides.  The portion of the shoreline that lies between the high and low tide lines is called the intertidal zone.  Intertidal ecosystems have high levels of sunlight, nutrients, and oxygen. The effects of tides

Section 3.2 Summary – pages The effects of tides  Intertidal zones differ in rockiness and wave action.  If the shore is rocky, waves constantly threaten to wash organisms into deeper water.

Section 3.2 Summary – pages  If the shore is sandy, wave action keeps the bottom in constant motion. The effects of tides

Section 3.2 Summary – pages  The photic zone of the marine biome includes the vast expanse of open ocean that covers most of Earth’s surface.  Most of the organisms that live in the marine biome are plankton. In the light

Section 3.2 Summary – pages In the light  Plankton are small organisms that drift and float in the waters of the photic zone.

Section 3.2 Summary – pages In the light  Plankton are important because they form the base of all aquatic food chains.  Baleen whales and whale sharks, some of the largest organisms that have ever lived, consume vast amounts of plankton.

Section 3.2 Summary – pages  Although the summer sun heats the surface of a lake the water a few feet below the surface remains cold.  These temperature variations within a lake are an abiotic factor that limits the kinds of organisms that can survive in deep lakes. Freshwater biomes

Section 3.2 Summary – pages Freshwater biomes  Another abiotic factor that limits life in deep lakes is light. Greatest Warmer layer Colder layer Least Greatest species diversity Oxygen and light penetration

Section 3.2 Summary – pages Other aquatic biomes  Other places where land and water meet are called wetlands, but there are several different kinds of wetlands. Swamps have trees.  Marshes do not, but both usually have water flowing through them.  Other wetland areas, called bogs, get their water supply from rain. Water does not flow through bogs.

Section 3.2 Summary – pages Terrestrial Biomes: Latitude and climate  Latitude describes your position in degrees north and south of the equator. O North pole South pole Sun’s rays Equator 66.5 o 23.5 o o 0

Section 3.2 Summary – pages Terrestrial Biomes: Latitude and climate  At different latitudes, the sun strikes Earth differently. O North pole South pole Sun’s rays Equator 66.5 o 23.5 o o 0

Section 3.2 Summary – pages  As a result, the climate — wind, cloud cover, temperature, humidity and precipitation in that area — are different. Terrestrial Biomes: Latitude and climate

Section 3.2 Summary – pages Terrestrial Biomes: Latitude and climate  Latitude and climate are abiotic factors that affect what plants and animals will survive in a given area. Annual precipitation (cm) Tundra Taiga Temperate forest Woodland Savanna Desert Tropical seasonal forest Tropical rain forest Temperate rain forest Average temperature ( o C) Annual Precipitation vs. Temperature for Various Biomes Grassland Shrubland

Section 3.2 Summary – pages Life on the tundra  The tundra is a treeless land with long summer days and short periods of winter sunlight.

Section 3.2 Summary – pages Life on the tundra  Because of its latitude, temperatures in the tundra never rise above freezing for long, and only the topmost layer of soil thaws during the summer.  Underneath this top layer is a layer of permanently frozen ground called permafrost.  The soil is lacking in nutrients.

Section 3.2 Summary – pages Life on the tundra  Lack of nutrients limits the types of organisms the tundra can support.  The short growing season limits the type of plants found in this biome to grasses, dwarf shrubs, and cushion plants.

Section 3.2 Summary – pages Life on the tundra  Hordes of mosquitoes and black-flies are some of the most common tundra insects during the short summer.  The tundra also is home to a variety of small mammals, including ratlike lemmings, weasels, arctic foxes, snowshoe hares, and even birds such as snowy owls and hawks.

Section 3.2 Summary – pages Life on the tundra  Musk oxen, caribou and reindeer are among the few large animals that migrate into the area and graze during the summer months.

Section 3.2 Summary – pages Life on the taiga  Just south of the tundra lies another biome that circles the north pole.  The taiga (TI guh) also is called the boreal or northern coniferous forest.

Section 3.2 Summary – pages  Common trees are larch, fir, hemlock, and spruce trees. Life on the taiga

Section 3.2 Summary – pages  Because of their latitude, taiga communities usually are somewhat warmer and wetter than tundra. Life on the taiga

Section 3.2 Summary – pages  The topsoil, which develops slowly from decaying coniferous needles, is acidic and poor in minerals.  However, the prevailing climatic conditions are still harsh, with long, severe winters and short, mild summers. Life on the taiga

Section 3.2 Summary – pages  More large species of animals are found in the taiga as compared with the tundra. Life on the taiga

Section 3.2 Summary – pages Life in the desert  The driest biome is the desert biome. A desert is an arid region with sparse to almost nonexistent plant life.

Section 3.2 Summary – pages  Deserts usually get less than 25 cm of precipitation annually. Life in the desert

Section 3.2 Summary – pages  With rainfall as the major limiting factor, vegetation in deserts varies greatly.  The driest deserts are drifting sand dunes. Life in the desert

Section 3.2 Summary – pages  The leaves of some desert plants curl up, or even drop off altogether, thus reducing water loss during extremely dry spells.  Many desert plants are annuals that germinate from seed and grow to maturity quickly after sporadic rainfall.  Many desert mammals are small herbivores that remain under cover during the heat of the day, emerging at night to forage on plants. Life in the desert

Section 3.2 Summary – pages  Coyotes, hawks, owls and roadrunners are carnivores that feed on the snakes, lizards, and small mammals of the desert. Life in the desert

Section 3.2 Summary – pages Life in the grassland  Grasslands are large communities covered with rich soil, grasses, and similar plants.

Section 3.2 Summary – pages  Grasslands, occur principally in climates that experience a dry season, where insufficient water exists to support forests.  Grasslands contain few trees per hectare. Life in the grassland

Section 3.2 Summary – pages  The soils of grasslands have considerable humus content because many grasses die off each winter, leaving byproducts to decay and build up in the soil.  At certain times of the year, many grasslands are populated by herds of grazing animals. Life in the grassland

Section 3.2 Summary – pages  Other important prairie animals include jack rabbits, deer, elk, and prairie dogs.  Many species of insects, birds, and reptiles, also make their homes in grasslands. Life in the grassland

Section 3.2 Summary – pages Life in the temperate forest  When precipitation ranges from about 70 to 150 cm annually in the temperate zone, temperate deciduous forests develop.

Section 3.2 Summary – pages  Temperate or deciduous forests are dominated by broad-leaved hardwood trees that lose their foliage annually.  The soil of temperate forests usually consists of a top layer that is rich in humus and a deeper layer of clay. Life in the temperate forest

Section 3.2 Summary – pages  The animals that live in the temperate deciduous forest include squirrels, mice, rabbits, deer, and bears. Life in the temperate forest

Section 3.2 Summary – pages  Many birds, such as bluejays, live in the forest all year long, whereas other birds migrate seasonally. Life in the temperate forest

Section 3.2 Summary – pages Life in rain forests  Temperate rain forests are found on the Olympic peninsula in Washington state and in other places throughout the world, such as South America, New Zealand, and Australia.  There are two types of rain forests in the world—the temperate rain forest and the more widely known tropical rain forest.

Section 3.2 Summary – pages  As their name implies, tropical rain forests have warm temperatures, wet weather, and lush plant growth. Life in rain forests

Section 3.2 Summary – pages  The average temperature is about 25 0 C. Life in rain forests

Section 3.2 Summary – pages  One reason for the large number of niches in rain forests is vertical layering.  Rain forests receive at least 200 cm of rain annually; some rain forests receive 600 cm. Life in rain forests

Section 3.2 Summary – pages  The tree tops are exposed to rain, sunlight, and strong winds.  The canopy layer, meters high, is a living roof.  A few giant trees called emergents pole through the canopy. A Tropical Rain Forest: Canopy

Section 3.2 Summary – pages A Tropical Rain Forest: Canopy  Birds, such as scarlet macaws, live on the fruits and nuts of the trees.  Monkeys frequently pass through.

Section 3.2 Summary – pages  Leaf cutter ants harvest leaves and bring them to the ground.  In the understory, the air is still, humid, and dark. Vines grow from the soil to the canopy.  Plants include ferns, broad-leaved shrubs, and dwarf palms. A Tropical Rain Forest: Understory

Section 3.2 Summary – pages  The limbs of the trees are hung with a thick layer of epiphytes, plants that get most of their moisture from the air.  Insects are common in the understory.  Birds and bats prey upon the insects. A Tropical Rain Forest: Understory

Section 3.2 Summary – pages  Reptiles include chameleons and snakes.  Tree frogs are common understory amphibians. A Tropical Rain Forest: Understory

Section 3.2 Summary – pages A Tropical Rain Forest: Ground  Leaves and other organic materials decay quickly.  The ground layer is a moist forest floor.  Roots spread throughout the top 18 inches of soil  There is great competition for nutrients.

Section 3.2 Summary – pages A Tropical Rain Forest: Ground  Ants, termites, earthworms, bacteria, and fungi live in the soil and quickly decompose organic materials.  Mammals living on the ground include rodents and cats, such as the jaguar.

Section 3.2 Summary – pages Life in rain forests  Some rain forest plants are important sources of medicinal products and hardwood trees and have provided a source of income for people.

Section 3.2 Summary – pages Life in rain forests  Agricultural land is not common in rain forests.

Section 3.2 Summary – pages Life in rain forests  Without organic matter, once rain forest soil is exposed and farmed, it becomes hard, almost brick-like, and nutrient-poor in a matter of a few years.  Soils in rain forests do not have substantial amounts of organic matter because leaf matter, which contains nutrients, disappears so quickly.